A QUASI-CRYSTALLINE MODEL OF DIFFUSION IN TERNARY LIQUID SYSTEMS

1965 ◽  
Vol 43 (6) ◽  
pp. 1812-1828 ◽  
Author(s):  
J. E. Lane ◽  
J. S. Kirkaldy

A quasi-crystalline model of a dilute ternary liquid system is proposed in which diffusion occurs by an interchange of species on neighboring lattice sites. Nonelectrolyte molecules are assumed to interchange with any type of diffusing species present in the system. In ternary nonelectrolyte systems relatively large cross-effects are associated with the mutual interchange of the two dilute solute species. The symmetry of the L-matrix arises directly through the application of detailed balance (microscopic reversibility) to this unit process.In electrolyte solutions, the only significant contribution to the ionic fluxes is expected to arise through interchange of ions with uncharged molecules. For diffusion in an aqueous solution of two strong electrolytes with a common ion, large off-diagonal L-coefficients result from the transformation of the lattice-referred diagonal diffusion matrix, written in terms of ionic fluxes and forces, to a form which relates the two independent salt fluxes and forces. Symmetry of the L-matrix in this case arises indirectly through the application of detailed balance to the ion-solvent interchanges. In aqueous electrolyte solutions the dilute solution ternary L-coefficients can be calculated from the independent individual ionic mobilities at infinite dilution, and these are found to be in excellent agreement with the experimental values for the system NaCl–KCl–H2O. The application of the model to binary electrolyte solutions at infinite dilution correctly yields the Nernst equation.The model is extended to solutions of two electrolytes with one or both incompletely ionized and to solutions containing a nonelectrolyte and a strong electrolyte. In all applications of the model the derived L-coefficients satisfy the well-known thermodynamic requirements. When appropriate ancillary data is available, the model yields fair to excellent predictions of the diffusion matrix at low concentrations of the solute species. Possible methods of improving the agreement at higher concentrations are discussed.

1987 ◽  
Vol 52 (7) ◽  
pp. 1672-1679 ◽  
Author(s):  
Ivan Horsák ◽  
Ivo Sláma

Based on the quasi-lattice concept, a simple model is proposed for calculating the quantities of mixing of strong electrolyte solutions over the whole concentration range from pure solvent to pure salt. This model is analogous to the regular solution model for non-electrolyte systems. Relationships for the activity coefficients of the solvent and salt have been derived, and the behaviour of the model in the limit of infinite dilution is discussed by comparison with the Debye-Huckel theory. The adequacy of equations derived from the proposed model has been tested by fitting published experimental data for the activities of water in the systems (Li, K)NO3-H2O and (Ag, Tl)NO3-H2O, which have been measured over the whole concentration range.


2005 ◽  
Vol 498-499 ◽  
pp. 49-54 ◽  
Author(s):  
Fábio de Oliveira Arouca ◽  
João Jorge Ribeiro Damasceno

The behavior of an isothermal and non-reaction solid-liquid system can be model using a mathematical model based on the Mixtures’ Theory of Continuum Mechanics. The knowledge of the constitutive equations of this phenomenon, as pressure on the solids and medium permeability, is very important in the design and performance evaluation of the continuous thickeners or filters. In this work the batch sedimentation phenomena of a kaolin aqueous suspensions was investigated. The technique consists on measuring of the gamma rays attenuation when they cross the physical media as a function of the local concentration at several vertical positions in a reservoir. Using the experimental data and local concentration as a function of the attenuation curve, it is possible to determine the constitutive equations. The results were satisfactory, allowing simulations of this phenomenon for steady and transient regimes in future papers.


1976 ◽  
Vol 54 (18) ◽  
pp. 2953-2966 ◽  
Author(s):  
Douglas E. Goldsack ◽  
Raymond Franchetto ◽  
Arlene (Anttila) Franchetto

The Falkenhagen–Leist–Kelbg equation for the conductivity of electrolyte solutions has been extended to include the effect of solvation on the concentration of the salt. Two equations have been derived, both of which have only two freely adjustable parameters at any temperature: Λ0 the molar conductance of the salt at infinite dilution and H0, a solvation number parameter for the salt. In one of these equations H0 is assumed to be independent of concentration. In the other, H0 is assumed to be dependent on concentration and an explicit concentration dependent formula is derived for H0. Conductance data for the alkali halide salts in the 0.5 to 10 m concentration range and 0 to 60 °C temperature range were found to be adequately reproduced by both these equations, but with the variable hydration parameter equation yielding better fits to the data. The H0 parameters from the fixed hydration parameter equation are found to be similar to those obtained from the analysis of activity coefficient and other data whereas the variable hydration parameter equation yields H0 parameters which are much larger.


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